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In thermodynamics and molecular chemistry, the enthalpy or heat content (denoted as H or ΔH, or rarely as χ) is a quotient or description of thermodynamic potential of a system, which can be used to calculate the "useful" work obtainable from a closed thermodynamic system under constant pressure.
   The term enthalpy is composed of the prefix en-, meaning to "put into", plus the Greek word -thalpein, meaning "to heat", although the original definition is thought to have stemmed from the word, "enthalpos" (ἐνθάλπος). It is often calculated as a differential sum, describing the changes within exo- and endothermic reactions, which minimize at equilibrium.

History

Over the history of thermodynamics, several terms have been used to denote what is now known as the enthalpy of a system. Originally, it was thought that the word "enthalpy" was created by Benoit Paul Émile Clapeyron and Rudolf Clausius through the publishing of the Clausius-Clapeyron relation in "The Mollier Steam Tables and Diagrams" in 1927, but it was later published that the earliest recording of the word was in 1875, by Josiah Willard Gibbs in the publication "Physical Chemistry: an Advanced Treatise", although it isn't referenced in Gibbs' works directly. In 1909, Keith Landler discussed Gibbs' work on the 'heat function for constant pressure' and noted that Heike Kamerlingh Onnes had coined its modern name from the Greek word "enthalpos" (ενθαλπος) meaning "to put heat into."

Original Definition

This is the heat change which occurs when 1 mol of a substance reacts completely with oxygen to form products at 298K and 1 atm. The function H was introduced by the Dutch physicist Heike Kamerlingh Onnes in early 20th century in the following form:
» H = E + pV,,

where E represents the energy of the system. In the absence of an external field, the enthalpy may be defined, as it's generally known, by:
» H = U + pV,,



where (all units given in SI)

Application and extended formula

Overview

In terms of thermodynamics, enthalpy can be calculated by determining the requirements for creating a system from "nothingness"; the mechanical work required, PV differs, based upon the constance of conditions present at the creation of the thermodynamic system. Internal energy, U, must be supplied to remove particles from a surrounding in order to allow space for the creation of a system, providing that environmental variables, such as pressure (p) remain constant. This internal energy also includes the energy required for activation and the breaking of bonded compounds into gaseous species.
   This process is calculated within enthalpy calculations as U + PV, to label the amount of energy or work required to "set aside space for" and "create" the system; describing the work done by both the reaction or formation of systems, and the surroundings. For systems at constant pressure, the change in enthalpy is the heat received by the system plus the non-mechanical work that has been done.
   Therefore, the change in enthalpy can be devised or represented without the need for compressive or expansive mechanics; for a simple system, with a constant number of particles, the difference in enthalpy is the maximum amount of thermal energy derivable from a thermodynamic process in which the pressure is held constant. The term pV is the work required to displace the surrounding atmosphere in order to vacate the space to be occupied by the system.

Relationships

As an expansion of the first law of thermodynamics, enthalpy can be related to several other thermodynamic formulae. As with the original definition of the first law; » mathrm ,

This expression is described by the diagram above.

Standard enthalpy changes

Definitions

Standard Enthalpy Change of Combustion Standard Enthalpy Change of Hydrogenation Standard Enthalpy Change of Formation Standard Enthalpy Change of Reaction A common standard enthalpy change is the standard enthalpy change of formation, which has been determined for a vast number of substances. The enthalpy change of any reaction under any conditions can be computed, given the standard enthalpy change of formation of all of the reactants and products. Other reactions with standard enthalpy change values include combustion (standard enthalpy change of combustion) and neutralisation (standard enthalpy change of neutralisation).

Examples: Inorganic compounds (at 25 °C)

Phase (matter)
Δ Hf0 in kJ/mol
Ammonia (Ammonium Hydroxide) aq -80.8
Ammonia g -46.1
Sodium carbonate s -1131
Sodium chloride (table salt) aq -407
Sodium chloride (table salt) s -411.12
Sodium chloride (table salt) l -385.92
Sodium chloride (table salt) g -181.42
Sodium hydroxide aq -469.6
Sodium hydroxide s -426.7
Sodium nitrate aq -446.2
Sodium nitrate s -424.8
Sulfur dioxide g -297
Sulfuric acid l -814
Silica s -911
Nitrogen dioxide g +33
Nitrogen monoxide g +90
Water l -286
Water g -241.8
Carbon dioxide g -393.5
Hydrogen g 0
Fluorine g 0
Chlorine g 0
Bromine l 0
Bromine g 0
» (State: g - gaseous; l - liquid; s - solid; aq = aqueous)

Specific enthalpy

The specific enthalpy of a working mass is a property of that mass used in thermodynamics, defined as h=u+p cdot v where u is the specific internal energy, p is the pressure, and v is specific volume. In other words, h = H/m where m is the mass of the system. The SI unit for specific enthalpy is joules per kilogram.

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